Weather Alert in Texas
High Wind Warning issued March 14 at 1:43AM CDT until March 14 at 7:00PM CDT by NWS San Angelo TX
AREAS AFFECTED: Fisher; Nolan; Sterling; Coke; Runnels; Irion; Tom Green; Concho; Haskell; Throckmorton; Jones; Shackelford; Taylor; Callahan; Coleman; Brown; McCulloch; San Saba
DESCRIPTION: * WHAT...West winds 35 to 45 mph with gusts up to 60 mph expected. * WHERE...A portion of west central Texas mainly north of a San Angelo to Brady line. * WHEN...From 7 AM this morning to 7 PM CDT this evening. * IMPACTS...Damaging winds will blow down trees and power lines. Power outages are expected. Travel will be difficult, especially for high profile vehicles.
INSTRUCTION: A High Wind Warning means that dangerously strong winds of at least 40 mph or gusts of 58 mph or higher are expected or occurring. Winds this strong will bring a threat to life and possibly cause property damage. Watch for downed trees and power lines. Secure loose outdoor objects. Expect hazardous driving conditions, especially for high profile vehicles. Caution should also be used if boating on area lakes due to choppy waters. People should avoid being outside in forested areas and around trees and branches. If possible, remain in the lower levels of your home during the windstorm, and avoid windows.
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds